Large regional anomalies have been revealed in the spectrum of the geomagnetic anomalous field in the Northern Pacific, and a schematic map of large regional anomalies has been compiled. It has been shown that large regional anomalies are located in the western part of the region (approximately up to 180–170° E), which has complicated geological, tectonic, and morphological structures and the oldest bottom rocks in the Pacific. Clear correlation of large regional magnetic anomalies with Δg anomalies of the same periodicity and with some particular anomalies revealed by MAGSAT satellites has been found.
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